The Pacific commercial advertiser. [volume] (Honolulu, Hawaiian Islands) 1885-1921, 1887-09-20
THE INDUSTRIAL SOUTH.
Inexhaustible Mineral Resources Tributary
to the City OF Chattanooga.

to the City of Chattanooga.
The soil of Chattanooga is fertile ir
iron. 1t underlies the very city, and
everywhere ribs the vast mountains
which surround it and stretch away or
every side as far as the eve can reach
But iron dug out of the ground is mixed
with impurities that need to be purgeC
away before it is fit for its multitudinous
uses. These auxiliary materials are
generally found at such distances from
the ore as to involve a heavy cost in
transportation. But in this section they
lie side by side and all together, the
iron with the coal needed for coke, the
limestone for smelling the ore. and the
tire-clay and sandstone for the construc-
ton of furnaces. An idea of these min
eral resources thus tributary to Chatta-
noOga can not better be given than in
the words of General John Z. Wilder,
the founder of the iron-worBs at Rock.
wood He says:
The coal-field of Tennessee extends
entirely across the State. from Kentucky
to Georgia and Alabama. being an ex-
tension of the Appalachian coal-felds,
whose northern extremity is in Northern
: Pennsylvania, and extends southwest
erly across Pennsylvania, West Vir-
ginia, Eastern Kentucky, Tennessee,
and ends in Central Alabama. The
coal-field of Tennessee covers 100
square miles; thel9 are about 4, 200
square miles in Alabama, and 25O
square miles in Georgia, all belonging
RI he & these
broad acres, excepting small area in
Alabama, form a covering for the Cum
berland table-land, raised above the
surrounding country, with an Outcrop
above the drainage of the valleys on
either side. easily opened, ventilated
and drained.
Throughout this extensive region are
wonderful beds of fossiliferous red
hematite iron ore, none of it more than
fifteen miles from the eastern outcrop
of the coal measures, and all of it
covered by the great limestone beds OF
the subcarboniferous period. ''All these
formations lie like the leaves of book,
fiat, bedded on each other, and general.
ly tilted up and broken into high ridges,
or folded into deep synclnal trOughs OF
valleys, in either case exposing the
edges of the ore beds, making it easy to
find, ready to mine, abundant in guam
tity, always accessible. These beds
usually average four or five feet in
thickness, sometimes more" The
General adds in regard to one species
of the timber of this region: 1.-The
largest forests of chestnut-oak in the
United States, producing the best
quality of tan-bark, cover the coal-fields
of Tennessee, Georgia and Alabama.
supplying the largest Oak-tannery on
the continent, at Chattanooga, and
furnishing tan-bark for the towns
of ST. Louis, Louisville and Gin
cinnati. They are sufficient in
area to supply 100000 cords per year
for an indefinite period without exhaus-
ton, as the tree reaches maturity in our
climate in forty years, and grows on an
area of over 10000 acres; and if cut
once in forty years, and producing only
two cords per tree, it would produce
perpetually $4,000 cords each year.
One cord of chestnut-oak tan-bark
grown in this latitude produces thirty
three per cent. more tannin than all the
bark grown north of the Kanawha
river"
Other woods equally valuable sur
round Chattanooga. The city is in the
midst of vast forest, where not one
sixth of the land has vet been subjected
to cultivation. Besides oak, there are
chestnut and black walnut standing
there in almost inexhaustible supply
a and primeval grandeur: Here too, is
continent and a sufficient supply of
red cedar is growing on the Clinch river
alone to furnish hOllOw-ware to every
American housekeeper for another cen
tury.-Harper''S Magazine.